Sunday, December 14, 2008
The Hubble Space Telescope has discovered carbon dioxide (CO2) in the atmosphere of a planet outside our solar system. The exoplanet HD 189733 b, roughly the mass of Jupiter, orbits a star 63 light-years away in extremely close company. Although the planet can't be seen directly, scientists used Hubble data to analyze its atmospheric composition and turn up CO2 as well as carbon monoxide (CO). They did this by comparing the light spectrum from the star with that from the star and planet combined, as the planet passes in front of its star. The very fact that we're able to detect it and estimate its abundance is significant for the long-term effort of characterizing planets both to find out what they are made of and if they could be a possible host for life. Other chemical signatures familiar to Earthlings have already been turned up by astronomical observations, including on HD 189733 b.
From this discovery it is possible that another planet might be able to host human beings due to the presence or carbon dioxide and monoxide in the atmosphere. Scientists will continue to test the atmosphere for other characterizations that could conclude another planet to be livable by humans.
Paragraph 1 a synopsis of article
Wednesday, December 10, 2008
Life on Other Planets?
The Nature of Glass Remains Anything but Clear
Tuesday, December 2, 2008
Early earth different than we knew it
Geologists now agree that Crystals in rocks that were found in Australia prove that the earth was not a desolate inhabitable place 4.5 billion years ago during the Hadean period. These crystals found embedded in rocks know as zircons are billions of years old and they offer signs that the Earth’s plate had begun shifting during the Hadean period. The minerals show that the plates were already forming continents and oceans 4.5 billion years ago. Zircons are composed of the elements Zirconium, oxygen, and silicon. They are really hard and durable and can survive harsh conditions that erode, melt, and destroy the rocks around them. The relative amounts of oxygen isotopes show that there was water. Zircons have high levels of oxygen-18 which in minerals in clays and carbonates that form in water prefer as well. The most common oxygen isotope is oxygen-16. Scientists believe the Earth at this time was a pretty placid place with both land and oceans. The temperatures on earth were cold enough to create large areas of lands covered by ice. The sun was much younger then and emitted 30 percent less energy then it does today.
http://www.nytimes.com/2008/12/02/science/02eart.html?ref=science
Silicon for better batteries
http://www.rsc.org/chemistryworld/News/2008/November/25110801.asp